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Geological Formation

Kittatinny Valley

Valleys

Kittatinny Valley is a section of the Great Appalachian Valley in northwestern New Jersey, lying between Kittatinny Mountain to the northwest and the New Jersey Highlands to the southeast, in Sussex and Warren counties. It is about 64 kilometers long and 16 to 21 kilometers wide, floored mainly by Martinsburg Formation shale and slate alongside Kittatinny and Jacksonburg limestone. The valley and its bordering ridge trace back to the Taconic Orogeny around 450 million years ago, when a volcanic island arc collided with proto-North America, with a later continental collision around 400 million years ago folding and faulting the rock into its present form. During the Wisconsin glaciation, ice up to 300 meters thick covered the valley and left behind end moraines, eskers, and lakes such as Culver's Lake and the 110-foot-deep Lake Aeroflex; today the Paulinskill, Wallkill, and Pequest rivers drain the valley. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/

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Caused By

Erosion, Processes

Wikidata P31 formation-type mapped to formative process Erosion via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Kittatinny Valley

In Discipline

Wikidata P31 formation-type mapped to discipline Geomorphology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Kittatinny Valley
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Also in Geography Atlas: where this subject is found.

Source Wikidata: Kittatinny Valley
Sources
Kittatinny Valley (Wikipedia)
Lead section
Quote, Lead section
The Kittatinny Valley is a section of the Great Appalachian Valley in Sussex and Warren counties in northwestern New Jersey that is bounded on the northwest by Kittatinny Mountain, and in the southeast by the New Jersey Highlands region.
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Wikidata: Kittatinny Valley
Wikidata Q6097470, class allow-list match (w-wdresolver-0926)View the Source
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